sedimentary

Chert (Holey Stone)

Microcrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness: 6.5–7 (Mohs); Color: Tan, brown, or buff; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Hardness: 6
Color: Tan, brown, or buff
Luster: Waxy to dull

Identified April 20, 2026More sedimentary →

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Physical properties

Hardness: 6.5–7 (Mohs); Color: Tan, brown, or buff; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Formation & geological history

Formed through the precipitation of silica within sedimentary rock layers, often replacing organic material or carbonate minerals. Many holey stones (hag stones) are formed through the abrasive action of water or boring organisms over thousands of years.

Uses & applications

Used historically for making tools or arrowheads due to its conchoidal fracture. Often kept as lucky charms (hag stones) or used in landscaping and aggregate.

Geological facts

Rocks with naturally occurring holes are often called 'Hag Stones' and have a rich history in European folklore for warding off spirits or protecting livestock.

Field identification & locations

Identify in the field by its hardness (will scratch glass), smooth waxy texture, and the presence of natural erosion holes. Commonly found on beaches or in stream beds.